РУДОНОСНОСТЬ ЗЕЯ-ГИЛЮЙСКОЙ СТРУКТУРЫ ЦЕНТРАЛЬНОГО ТИПА
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dc.contributor.author | Степанов В.А. | ru_RU |
dc.contributor.author | Мельников А.В. | ru_RU |
dc.contributor.author | Носырев М.Ю. | ru_RU |
dc.contributor.author | Дементиенко А.И. | ru_RU |
dc.date.accessioned | 2019-03-04T01:43:34Z | |
dc.date.available | 2019-03-04T01:43:34Z | |
dc.date.issued | 2009 | |
dc.identifier.citation | Вестник АмГУ, 2009, Выпуск 47 | ru_RU |
dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/1598 | |
dc.description.abstract | Within the limits of the Upper Priamyrye and according to geomorphologic, geological and geophysical facts, it was founded the separation of Zeya-Gilyuiskaya central type’s structure (CTS) according. It was shown that it is the through-crusted structure of ancient layer which have passed the series of activation stages, mostly of Mesozoic age. Ore-bearing process of CTS was characterized, deposits of gold, copper, nickel, graphite and other minerals regularly take place within the bounds of this structure, also there were founded diamonds’ grains. It’s supposed that platinum- and gold-ore copper-nickel mineralization, gold placers, graphite deposits and diamonds’ discovery have the most practical importance. | ru_RU |
dc.language | Русский | ru_RU |
dc.relation.ispartof | ВЕСТНИК АМУРСКОГО ГОСУДАРСТВЕННОГО УНИВЕРСИТЕТА. СЕРИЯ: ЕСТЕСТВЕННЫЕ И ЭКОНОМИЧЕСКИЕ НАУКИ | ru_RU |
dc.subject | РУДОНОСНОСТЬ СТРУКТУР | ru_RU |
dc.subject | ГЕОЛОГИЧЕСКОЕ СТРОЕНИЕ СТРУКТУР | ru_RU |
dc.subject | ГЕОФИЗИЧЕСКИЕ ПОЛЯ | ru_RU |
dc.subject | МАГНИТНЫЕ АНОМАЛИИ | ru_RU |
dc.subject | СТРУКТУРЫ ЦЕНТРАЛЬНОГО ТИПА | ru_RU |
dc.subject | МЕДНО-НИКЕЛЕВОЕ ОРУДЕНЕНИЕ | ru_RU |
dc.subject | МЕСТОРОЖДЕНИЯ | ru_RU |
dc.subject | РОССЫПИ ЗОЛОТА | ru_RU |
dc.subject | РУДНЫЕ ТЕЛА | ru_RU |
dc.subject | ГРАФИТОНОСНЫЕ УЗЛЫ | ru_RU |
dc.title | РУДОНОСНОСТЬ ЗЕЯ-ГИЛЮЙСКОЙ СТРУКТУРЫ ЦЕНТРАЛЬНОГО ТИПА | ru_RU |
dc.type | Статья, тезисы доклада | ru_RU |
dc.author.corporate | Институт геологии и природопользования ДВО РАН | ru_RU |